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Books on the topic 'Subduction plate'

Author: Grafiati
Published: 4 June 2021
Last updated: 10 February 2022

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1

Fukatai to kyodai jishin hasseitai: Nankai jishin no kaimei ni mukete. Tōkyō: Tōkyō Daigaku Shuppankai, 2009.

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2

1945-, Taniguchi Hiromitsu, ed. Magmatic response to the late phanerozoic plate subduction beneath East Asia. Sendai-shi: Tōhoku Daigaku Tōhoku Ajia Kenkyū Sentā, 2006.

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3

L, Smellie J., ed. Volcanism associated with extension at comsuming plate margins. London, England]: The Society, 1994.

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4

Deformation and exhumation at convergent margins: The Franciscan subduction complex. Boulder, Colo: Geological Society of America, 2008.

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5

D, Ryan Paul, and SpringerLink (Online service), eds. Arc-Continent Collision. Berlin, Heidelberg: Springer-Verlag Berlin Heidelberg, 2011.

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6

Tregoning, Paul. GPS measurements in the Australian and Indonesian regions, 1989-1993: Studies of the Java Trench subduction zone, the Sunda Strait and the Australian Plate. Sydney: School of Geomatic Engineering, University of New South Wales, 1996.

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7

Active Tectonics Of The Hellenic Subduction Zone. Springer, 2012.

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8

Eichelberger, John, Evgenii Gordeev, Pavel Izbekov, Minoru Kasahara, and Jonathan Lees. Volcanism and Subduction: The Kamchatka Region. American Geophysical Union, 2013.

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9

Eichelberger, John, Evgenii Gordeev, Pavel Izbekov, Minoru Kasahara, and Jonathan Lees. Volcanism and Subduction: The Kamchatka Region. American Geophysical Union, 2013.

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10

Eichelberger, John, Evgenii Gordeev, Pavel Izbekov, Minoru Kasahara, and Jonathan Lees. Volcanism and Subduction: The Kamchatka Region. American Geophysical Union, 2013.

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11

E, Wells Ray, and Geological Survey (U.S.), eds. Cascadia: Regional lithospheric studies of the Pacific Northwest. [Menlo Park, CA]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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12

Van Hinsbergen, Douwe J. J., Edwards M. A, Govers Rob 1961-, and Geological Society of London, eds. Collision and collapse at the Africa-Arabia-Eurasia subduction zone. London, UK: Geological Society, 2009.

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13

L, Smellie J., and Geological Society of London, eds. Volcanism association with extension at consuming plate margins. London: Geological Society, 1998.

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14

Wakabayashi, John, and Yildirim Dilek, eds. Plate Tectonics, Ophiolites, and Societal Significance of Geology: A Celebration of the Career of Eldridge Moores. Geological Society of America, 2021. http://dx.doi.org/10.1130/spe552.

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This volume honors Eldridge Moores, one of the most accomplished geologists of his generation. The volume starts with a summary of Moores’ achievements, along with personal dedications and memories from people who knew him. Leading off the volume’s 12 chapters of original scientific contributions is Moores’ last published paper that presents an example of the Historical Contingency concept, which suggested that earlier subduction history may result in supra-subduction zone geochemical signatures for some magmas formed in non-subduction environments. Other chapters highlight the societal significance of geology, the petrogenesis of ophiolites, subduction zone processes, orogenic belt evolution, and other topics, covering the globe and intersecting with Moores’ interests and influences.
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15

Volcanism associated with extension at consuming plate margins. London: Geological Society, 1994.

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16

Ludwig, Rainer. Double subduction beneath Hispaniola?: An investigation of earthquakes by body wave inversion. 1989.

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17

Renata, Dmowska, and Ekström Göran, eds. Shallow subduction zones: Seismicity, mechanics, and seismic potential. Basel: Birkhäuser Verlag, 1993.

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18

Dmowska, R., and G. Ekstrom. Shallow Subduction Zones: Seismicity, Mechanics and Seismic Potent. Birkhauser, 1993.

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19

Driving Force of Tectonic Plate. Cres Huang, 2015.

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20

C, Zoback Mary Lou, and Geological Survey (U.S.), eds. Wellbore breakout analysis for determining tectonic stress orientations in Washington State. Menlo Park, Calif: U.S. Dept. of the Interior, U.S. Geological Survey, 1992.

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21

Fabritius, R. Axel. Shear-wave anisotrophy across the Cascadia Subduction Zone from a linear seismograph array. 1995.

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22

Fabritius, R. Axel. Shear-wave anisotrophy across the Cascadia Subduction Zone from a linear seismograph array. 1995.

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23

Wahrhaftig, Clyde. Streetcar to Subduction and Other Plate Tectonic Trips by Public Transport in San Francisco. Amer Geophysical Union, 1985.

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24

(Editor), M. Cloos, W. D. Carlson (Editor), M. C. Gilbert (Editor), J. G. Liou (Editor), and S. S. Sorensen (Editor), eds. Convergent Margin Terranes and Associated Regions: A Tribute to W.G. Ernst Special Paper 419. Geological Society of Amer, 2007.

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25

(Editor), Timothy B. Byrne, and Char-Shine Liu (Editor), eds. Geology and Geophysics of an Arc-Continent Collision, Taiwan (Special Paper (Geological Society of America)). Geological Society of America, 2002.

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26

Ryan, Paul D., and Dennis Brown. Arc-Continent Collision. Springer, 2016.

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27

DMOWSKA and ECKSTRÖM. Shallow Subduction Zones: Seismicity, Mechanics and Seismic Potential Part 1 (Pageoph Topical Volumes). Birkhauser, 1993.

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28

Gurūpu, Kaikō II Kenkyū, ed. Nihon shūhen no kaikō: 6000m no shinkaitei e no tabi : shashinshū = 6000 meters deep : a trip to the Japanese trenches ; photographic records of the Nautile Dives in the Japanese subduction zones. Tōkyō: Tōkyō Daigaku Shuppankai, 1987.

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29

Kantaro, Fujioka, and Kaiko (Project), eds. A moins 6000m: L'exploration des fosses japonaises : photographies des plongées du submersible Nautile dans les fosses de subduction du Japon. Tokyo: IFREMER/CNRS/University of Tokyo Press, 1988.

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30

Livermore, Roy. Continents and Supercontinents. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198717867.003.0008.

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Keith Runcorn’s boys showed beyond any doubt that the continents had been touring the globe since the Precambrian, long before they converged on Pangea. Their precise pre-Pangea itineraries were, however, uncertain, for while the ancient latitude of each block could be determined from the magnetic dip of suitable rock samples of the correct age (assuming such could be found), the ancient longitude was a different matter. The magnetic compass in ancient rocks recorded the direction to the ancient pole, but did not allow continents to be placed in their correct relative longitudes. Worse still, the best evidence of relative plate motions—marine magnetic anomalies and fracture zones—had all been shredded by subduction during the assembly of Pangea. And, since the old continents had been around the block a bit since the Paleozoic, there were no continental margins that you could fit together, as had been done for the Atlantic continents by Teddy Bullard and colleagues. Geologists were left only with indirect evidence from rock outcrops to guess the relative positions of these earlier continents. On the bright side, however, the lack of constraints freed them to give full reign to their imaginations, and they quickly began postulating lost supercontinents of all kinds.
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